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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/119915
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dc.contributor.authorYong, C. K.-
dc.coverage.spatialAdelaide Geosyncline, Mount Lofty Ranges, South Australia-
dc.date.issued1964-
dc.identifier.urihttp://hdl.handle.net/2440/119915-
dc.descriptionThis item is only available electronically.en
dc.description.abstractThe area of uniform stratigraphic sequence studied is essentially part of the west limb of a regional anticlinorium. Both the mesoscopic and the macroscopic folds have the same concentric style. Two different explanations are suggested for the apparently odd occurrence of a 30-foot arkosic quartzite band near the top of the northern foothills.en
dc.language.isoenen
dc.subjectHonours; Geology; Adelaide Geosyncline; Adelaidean; stratigraphy; structureen
dc.titleGeology of the Mt. Osmond area, South Australiaen
dc.typeThesisen
dc.contributor.schoolSchool of Physical Sciencesen
dc.provenanceThis electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legalsen
dc.description.dissertationThesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1964-
Appears in Collections:School of Physical Sciences

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